{"refrec":{"BRefID":252917,"RR":"<b>Cole, A.R.; Harris, P.T.; Keene, J.B.</b> (1995). Foraminifers as facies indicators in a tropical, macrotidal environment: Torres Strait-Fly River delta, Papua New Guinea, <b><i>in</i></b>: Flemming, B.W. <i>et al.</i> (Ed.) <i>Tidal Signatures in Modern and Ancient Sediments. Special Publication of the International Association of Sedimentologists,</i> 24: pp. 213-223","BEntID":244731,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Flemming, B.W. <i>et al.</i> <i>Tidal Signatures in Modern and Ancient Sediments. Special Publication of the International Association of Sedimentologists,</i> 24: pp. 213-223","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Cole, A.R.; Harris, P.T.; Keene, J.B.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Cole, A.R. <i>et al.</i>","Englishabstract":"Foraminifer assemblages are assessed as potential recorders of transportation and redistribution by tidal processes in tropical, tidally dominated carbonate shelf and fluvio-deltaic environments. Four facies are identified on the basis of grain-size distribution, carbonate content and energy: (i) a high energy carbonate sand facies; (ii) a low energy muddy carbonate sand facies; (iii) a transitional mixed terrigenous and carbonate sediment facies; and (iv) a terrigenous delta front facies. Up to 1300 tests were picked from nine representative samples and analysed using a computerized image analysis system. This method allowed the determination of maximum and minimum test dimensions, as well as two-dimensional shape and area, to produce a grain-size histogram of foraminifer tests for each site. The results show that each of the four facies can be identified from the combination of foraminiferal taphonomic and grain-size properties. Furthermore, such properties identified the mode of transport (i.e. suspension versus bedload) and transport pathways at the sample locations. A small amount of carbonate material is transported landwards in suspension and deposited among the mostly (>95%) terrigenous sediments comprising the prograding Fly delta. 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